The reception of ground-based Loran transmissions by the fixed-frequency topside sounder satellite

Details The reception of ground-based Loran transmissions by the fixed-frequency topside sounder satellite The reception of ground-based Loran transmissions by the fixed-frequency topside sounder satellite

Nov 1967

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1967jatp...29.1383l&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 29, no. 11, pp. 1383-1386, IN9

Physics

1

Scientific paper

Transmissions from ground-based Loran stations have frequently been detected by the 2 MHz receiver on the Explorer 20 satellite; the form of the resultant interference permits the identification of individual Loran transmitters. A statistical study of the occurrence of the interference on passes recorded at Winkfield in the United Kingdom suggests that it is due to an E-W trough of low critical frequency at latitudes between about 55°N and 65°N at western European longitudes; this trough may be associated with the trough of low electron density observed over Canada by Muldrew.

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